Crozier Mine

Past Producer in Augusta county in Virginia, United States with commodity Iron
Sections on this page
  1. Identification information
  2. Geographic coordinates
  3. Site location context
  4. Geographic areas
  5. Commodities
  6. Materials information
  7. Host and associated rocks
  8. Nearby scientific data
  9. Geologic structures
  10. Ore body information
  11. Economic information about the deposit and operations
  12. Land status
  13. Workings at the site
  14. Links to other databases
  15. Bibliographic references
  16. General comments
  17. Reporter information

Geologic information

Identification information

Deposit ID 10080680
MRDS ID W032017
Record type Site
Current site name Crozier Mine

Geographic coordinates

Geographic coordinates: -79.12586, 38.05588 (WGS84)
Elevation 529
Relative position 6.4 KM (4 MI) NORTHEAST OF GREENVILLE AND 2.8 KM (1.75 MI) SOUTHWEST OF MINT SPRING.

Site location context

Political divisions (FIPS codes)

Augusta(county)

Virginia(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Greenville(quadrangle 1:24,000 scale)

Staunton(quadrangle 1:100,000 scale)

Charlottesville(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

South Fork Shenandoah(hydrologic unit)

Potomac(hydrologic accounting unit)

Potomac(hydrologic subregion)

Mid Atlantic(hydrologic region)

Geographic areas

Country State County
United States Virginia Augusta

Comments on the location information

  • 1.4 KM (0.9 MI) NORTH ON U.S. ROUTE 11 FROM ITS WESTERN INTERSECTION WITH STATE ROAD 694, TURN WEST ON GRAVEL DRIVE FOR ABOUT 0.4 KM (0.25 MI), CONTINUE NORTHWEST INTO WOODS FOR 210 M (689 FT) TO TOP OF RIDGE: MINE IS ABOUT 91.5 TO 137 M (300 TO 450 FT) NORTHEAST OF HOUSE ON THE RIDGE CREST.

Commodities

Commodity Importance
Iron Primary

Comments on the commodity information

  • IRON ORE CLASSIFIED AS MOUNTAIN BROWN ORE.

Materials information

Materials Type of material
Goethite Ore
Limonite Ore

Host and associated rocks

  • Host or associated Host
    Rock type Sedimentary Rock > Carbonate > Limestone
    Rock unit name Beekmantown Formation
    Rock description Beekmantown Formation
    Stratigraphic age (youngest) Late Ordovician
    Stratigraphic age (youngest) Late Ordovician
  • Host or associated Host
    Rock type Sedimentary Rock > Carbonate > Dolomite

Nearby scientific data

(1) Elbrook Formation

Economic information

Geologic structures

Type of structure Regional
Structure description Ne-Sw Trend, Massanutten Synclinorium
Type of structure Local
Structure description Pulaski-Staunton Fault Lies 2 Km (1.4 Mi) To The Nw: Fairfield Fault Lies 1.4 Km (0.85 Mi) To The Se.

Ore body information

  • General form IRREGULAR POCKETS

Economic information about the deposit and operations

Development status Past Producer
Commodity type Metallic
Deposit size Small
Significant No
Discovery year 1900
Year of first production 1900
Year of last production 1900

Land status

Ownership category Private

Workings at the site

  • Type of workings Surface/Underground
    Overall depth 8M

Comments on the workings information

  • 1 SHAFT AND FOUR PITS WERE SEEN IN 1981. THE SHAFT IS ABOUT 8 M (25 FT) DEEP AND IS REPORTED TO HAVE HAD SEVERAL DRIFTS. THE PITS AVERAGED 2.4 M (8 FT) IN DIAMETER AND 1 M (3 FT) IN DEPTH.

Comments on development

  • MINE WAS OPERATED NEAR THE END OF THE NINETEENTH CENTURY.

Reference information

Bibliographic references

  • Deposit

    RADAR, E.K., 1967, GEOLOGY OF THE STAUNTON, CHURCHVILLE, GREENVILLE, AND STUARTS DRAFT QUADRANGLES, VIRGINIA: VDMR REPT OF INVESTIGATION 12, 43 P.

  • Deposit

    HARDER, E.C., 1909, THE IRON ORES OF THE APPALACHIAN REGION IN VIRGINIA: USGS BULL 380, PP.215-254.

General comments

Subject category Comment text
Deposit ORE ROCKS FOUND NEAR THE OPENING APPEAR TO BE OF A WEATHERED HIGH-GRADE MATERIAL. DEPOSIT CONSISTS OF ANGULAR FRAGMENTS OF VARIOUS SIZES AND FORMS SCATTERED THROUGH VARIEGATED OR BROWN CLAYS. THE FRAGMENTS WERE PROBABLY AT ONE TIME PARTS OF LARGER MASSES, WHICH HAVE BEEN BROKEN UP BY THE SLUMPING OF THE CLAY.THESE MASSES WERE MOSTLY SMALL VEINS AND REPLACEMENTS ALONG LINES OF FRACTURE OR BEDDING PLANES. HERE AND THERE FRAGMENTS ARE GROUPED IN LITTLE POCKETS, AND IN SUCH PLACES THEY WERE PROBABLY ORIGINALLY PARTS OF SMALL DISCONNECTED MASSES. THE LIMONITE IS BROWN, EARTHY, AND AMORPHOUS.

Reporter information

Type Date Name Affiliation Comment
Reporter 01-MAY-1981 Trimble, David C. (Sweet, Palmer C.) Virginia Division of Mineral Resources

Beyond USGS

Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.